On the attribution of the impacts of extreme weather events to anthropogenic climate change

被引:57
作者
Perkins-Kirkpatrick, S. E. [1 ,2 ]
Stone, D. A. [3 ]
Mitchell, D. M. [4 ,5 ]
Rosier, S. [3 ]
King, A. D. [6 ]
Lo, Y. T. E. [4 ,5 ]
Pastor-Paz, J. [7 ]
Frame, D. [8 ]
Wehner, M. [9 ]
机构
[1] UNSW Canberra, Sch Sci, Canberra, ACT, Australia
[2] UNSW Sydney, ARC Ctr Excellence Climate Extremes, Sydney, NSW, Australia
[3] NIWA, Wellington, Aotearoa, New Zealand
[4] Univ Bristol, Sch Geog Sci, Bristol, Avon, England
[5] Univ Bristol, Cabot Inst Environm, Bristol, Avon, England
[6] Univ Melbourne, Sch Geog Earth & Atmospher Sci, Melbourne, Vic, Australia
[7] Geol & Nucl Sci Inst GNS Sci, Wellington, New Zealand
[8] Victoria Univ Wellington, New Zealand Climate Change Res Inst, Wellington, New Zealand
[9] Lawrence Berkeley Natl Lab, Berkeley, CA USA
基金
澳大利亚研究理事会;
关键词
impacts; attribution; climate and weather extremes; climate change; RISK; HEATWAVE; RAINFALL; ENGLAND;
D O I
10.1088/1748-9326/ac44c8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Investigations into the role of anthropogenic climate change in extreme weather events are now starting to extend into analysis of anthropogenic impacts on non-climate (e.g. socio-economic) systems. However, care needs to be taken when making this extension, because methodological choices regarding extreme weather attribution can become crucial when considering the events' impacts. The fraction of attributable risk (FAR) method, useful in extreme weather attribution research, has a very specific interpretation concerning a class of events, and there is potential to misinterpret results from weather event analyses as being applicable to specific events and their impact outcomes. Using two case studies of meteorological extremes and their impacts, we argue that FAR is not generally appropriate when estimating the magnitude of the anthropogenic signal behind a specific impact. Attribution assessments on impacts should always be carried out in addition to assessment of the associated meteorological event, since it cannot be assumed that the anthropogenic signal behind the weather is equivalent to the signal behind the impact because of lags and nonlinearities in the processes through which the impact system reacts to weather. Whilst there are situations where employing FAR to understand the climate change signal behind a class of impacts is useful (e.g. 'system breaking' events), more useful results will generally be produced if attribution questions on specific impacts are reframed to focus on changes in the impact return value and magnitude across large samples of factual and counterfactual climate model and impact simulations. We advocate for constant interdisciplinary collaboration as essential for effective and robust impact attribution assessments.
引用
收藏
页数:9
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